5 minute read
Deep
The Wonders of a Frozen Landscape
Photos and story by Carrie Deegan
It’s that time of year again: the time when mere mortals can walk on water. Frozen water, sure, but it’s still one of the coolest (pun intended) feats of the season. There is something magical about sliding, skiing, skating, or snowshoeing out onto a frozen pond, exploring islands and coves you’ve reached by boat in the summer, except now you can just walk there like you’re heading to the mailbox. In my family, we wait not-so-patiently for those few perfect smooth ice days when we can slide out some goals and challenge friends to a spirited game of pond hockey Even when there is snow cover, frozen lakes and ponds provide unlimited winter fun. Where else can you cross-country ski or snowshoe for hours, enjoying expansive views without all those exhausting New Hampshire hills? Or pounce on a triggered tip-up and pull a fat perch up through the ice? In recent years, local Nordic skating enthusiasts have been plowing ice skating trails on many of our lakes, revealing miles of beautiful glassy ice for recreation even after all the lakes are snowbound
Opposite page: The author’s hockey skates make tracks on Mascoma Lake in Enfield, N H , last winter
Top: Kids enjoy a Nordic skating trail on Kezar Lake in Sutton, N.H., in 2021. Trails maintained for Nordic skating, where skate blades are attached via bindings to crosscountry ski boots, can also be enjoyed by anyone with hockey or figure skates.
Bottom: Family and friends play pond hockey on Otter Pond in New London, N.H. New Hampshire hosts several pond hockey tournaments, including the New England Pond Hockey Classic, which had to be moved from Lake Winnipesaukee to Lake Waukewan in 2023 due to unsafe ice conditions
Frozen lakes and ponds are truly part of the quintessential winter experience in New Hampshire, but how does it happen? When the air temperature drops in the fall, water at the surface of lakes also cools. Cool water is denser than warm, so the cooled surface water sinks toward the bottom of the lake, exposing warmer water above to the cool air again The process repeats until the entire water column is a uniform density and temperature of 39°F (4°C), the “magic” temperature when water is at its densest. This is a critical point in the seasonal cycle of any lake, as the uniform density allows the entire lake to mix, which is called fall turnover, distributing dissolved oxygen and important nutrients throughout the water column. It’s also a point that must be reached in order for the lake to freeze over Dropping below 39°F, surface water molecules now become less dense, arranging themselves into a lattice-like crystalline structure with a lower density than the liquid water below The resulting ice floats instead of sinking to the bottom!
The fact that frozen water floats instead of sinking is noteworthy because most liquids do not behave this way (bonus activity: try freezing a cube of olive oil and dropping it into a cup of liquid olive oil), but also because this allows aquatic life to persist under lake ice. Life under the ice isn’t easy Ice effectively seals the lake off like a big Tupperware lid, preventing gas exchange with the atmosphere and resulting in a steady decline in dissolved oxygen Light levels also decrease, especially with snow cover, limiting photosynthesis by aquatic plants, which further reduces oxygen, and reducing visibility for those animals that navigate and feed using sight.
Left: Children gather around a tip-up at an ice fishing demonstration day.
Bottom: Water pools on the ice surface of Little Lake Sunapee in New London, N.H., following a rain event in 2022.
Despite the challenges, aquatic animals and plants in our region have evolved to persevere in frozen lakes Plants often die back significantly, but many have thick, starchy roots that store energy for new growth in the spring or develop specialized winter buds (turions) that resist decay and store carbohydrates that allow the plant to clone itself when conditions improve Some aquatic animals endure the winter months by entering a state of dormancy Turtles and frogs bur y themselves in lake bottom sediments, or rest there in a state of torpor. Amazingly, these creatures can absorb dissolved oxygen through their skin, or persist at near-zero blood oxygen levels for months Fish, on the other hand, typically need to move at least slightly in order to pass water over their gills and absorb oxygen Warmer water specialists such as bass and bluegill seek out the calm, slightly warmer water near the bottom and remain quiescent, reducing their movement and metabolism to conser ve energy Others, including chain pickerel and yellow perch, are better adapted to the cold and slightly more active Ice anglers know that these species are easy to tempt into biting a hapless minnow under the ice Still other fish species are true winter specialists: lake trout and landlocked salmon are undeterred by cold temperatures, even seeking out the coldest water just under the ice since it holds more oxygen
Lake ice may seem an inviolable reality of winter, but we should not take it for granted There is ample evidence our ice cover is getting thinner and shorter in duration because of climate warming. A recent State of NH lake trends report revealed that “ice out” dates (the day that lakes fully thaw in spring) for 31 of our lakes are averaging about 2 weeks earlier than in the 1930s Instead of early May, we now expect ice out (which, incidentally, is the second time of year that oxygen and nutrients can mix freely throughout the water column) to occur in mid-April Even more disturbing, scientists have predicted that as many as 5,600 Northern Hemisphere lakes that now consistently freeze over will cease to do so by the end of this century. Larger and deeper lakes are most vulnerable, since it takes a longer stretch of consistently cold air temperatures to chill the entire water column Thankfully, New Hampshire’s lakes are still freezing, but several in neighboring states (e.g. Lake Sebago in Maine and Lake Champlain in Vermont) now freeze over during fewer than 50 percent of our winters
What will the consequences be if our lakes no longer freeze in winter? Economic and social repercussions we can quantify, with the loss of ice-related recreational opportunities like snow- mobiling and ice fishing But ecologically, we aren’t entirely sure Aquatic ecosystems have been studied most thoroughly in the warmer months, and much remains unknown about how trophic food webs, water chemistr y, and species diversity will react if our lakes don’t achieve seasonal turnover and freeze over. Some predictions include warmer summer water temperatures leading to more frequent algal blooms, issues with oxygen depletion near lake bottoms if spring and fall turnover do not occur, and loss of those species most highly adapted to cold water. On the bright side, scientific models also predict that we can significantly slow or even maintain ice loss at current levels if we’re able to curb greenhouse gas emissions and maintain colder winter air temperatures.
If you head out on the ice this winter, enjoy the experience, and be safe. New Hampshire Fish & Game has some helpful ice safety tips and best practices at https://www.wildlife.state.nh.us/ outdoor-recreation/ice-safety html While you’re out there, take a few moments to appreciate all the life and sur vival going on beneath that layer of frozen water under your feet Learning about the changes already facing New Hampshire’s lakes is the first step to taking action and supporting policies that will result in a solid future for our lake and pond ice